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LOCAL EARTHQUAKE HISTORY

Hachijo Town earthquake and Shindo history in 2016

八丈町

This annual view includes only earthquakes from 2016 for which stations associated with Hachijo Town recorded Shindo.

Data period: 1 January–31 December 2016
Data period: 1 January–31 December 2016

In 2016, stations associated with Hachijo Town reported local Shindo for 4 earthquakes. The highest local level recorded that year was Shindo 1.

Observed events42016
Highest local Shindo12016
Data period: 1 January–31 December 2016 · 4 observed earthquakes

Observation history · 2016

This history counts earthquakes observed at stations in the place, not earthquakes whose epicentre lies inside its boundary. Counts can change as stations are updated and older or corrected observations are added.

2016 · Clear filters
First observation: Jan 24, 2015

Observed events by year

Choose a year to update the event history and local Shindo distribution.

All years
2016

Shindo observed in this place

The highest reading from stations in this place, not the maximum Shindo of the whole event.

All Shindo
142030405−05+06−06+070
Reference model · not a forecast

Ground & J-SHIS

The context below uses the place's full available history and reference models; it is not part of the 2016 statistics.

Local seismic profile

Where the shaking usually comes from

Source regions of earthquakes observed here, ordered by the number of reports.

4
Adjacent Sea of Hachijojima Island八丈島近海
48
3
Off the east Coast of Hachijojima Island八丈島東方沖
40
2
Adjacent Sea of Miyakejima Island三宅島近海
4
2
Off the southeast Coast of Chiba Prefecture千葉県南東沖
3
2
Off the Coast of Fukushima Prefecture福島県沖
3
1
Adjacent Sea of Torishima Island鳥島近海
3
Reference model · not a forecast J-SHIS (NIED) · 250 m · 4939563332

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 八丈町三根.

J-SHIS / NIED

How to read these values

Landform classVolcanic footslope火山山麓地

A landform class assigned to the whole 250 m mesh and used to estimate AVS30. The name alone does not determine safety, and it is model data rather than a borehole survey at the station.

AVS30284.6 m/s

The average speed of an S-wave through the upper 30 metres. A lower value generally indicates softer material that can amplify shaking more. J-SHIS uses this value to estimate the amplification shown to the right. It is not predicted Shindo.

Surface velocity amplification×1.34

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 34% higher than at engineering bedrock (Vs = 400 m/s). This value describes motion velocity—it does not multiply magnitude or forecast ground acceleration.

Ground conditions can change over short distances. These values do not rate the whole place or the safety of a building, and they cannot predict an earthquake. Source: J-SHIS (NIED), V4 model; processed for presentation by JISHINDESU.

Local seismic profile

Nearby places

Municipalities nearest to the representative station position.